PSN-L Email List Message

Subject: RE: Iris Waveform Chart
From: "Jorma Kanninen" jorma@.............
Date: Sat, 5 Feb 2005 23:34:31 +0000


Hi Tim,

Now I'm getting a bit puzzled !

Cheers,

Jorma




From: psn-l-request@.............. [mailto:psn-l-request@webtroni=
cs.com] On Behalf Of Timothy Carpenter
Sent: 05 February 2005 21:33
To: psn-l@..............
Subject: RE: Iris Waveform Chart


I should probably know =96 but I don't. What is the "caustic" dis=
tance? And for that matter, what is the "caustic"?
Regards,
-Tim-

Timothy Carpenter, P.E., Pres.,
GeoDynamics Consultants, Inc.
5043 Whitlow Ct.
Commerce Twp., Mi 48382
248-363-4529 (voice & fax)
248-766-1629 (cell)
geodynamics@........... (primary)
geodynamics@....... (secondary)


-----Original Message-----
From: psn-l-request@.............. [mailto:psn-l-request@webtroni=
cs.com] On Behalf Of Connie and Jim Lehman
Sent: Sunday, January 09, 2005 7:03 PM
To: psn-l@..............
Subject: Iris Waveform Chart

PSN--thanks for the Iris Waveform Chart for the 9.0 Sumatra  12/2=
6/04 event.  The surface wave arrivals of multiple stations exhib=
ited by distance, and text,  makes a super graphic.  I was wonder=
ing about  the occurrence of a seismic caustic at the appropriate=
 degree distance.  Was the gap at 160 degree area due to no repor=
ting station near the "caustic" distance.  In periodic recording=20=
here we've copied three caustics  in 20 years--I believe the even=
ts were southwest of Australia for us--not a very hot spot.
    The 18 sec long period system at James Madison Un.  (Virginia=
) working into a graphic readout read the 8.1 Macquarie Is. event=
-(l2/23) nicely, but the 9.0 event read 20 min after P-diff arriv=
ed and then went off scale for 100 minutes and returned to normal=
 recording for the 7.1 event at 04:21.  One can conclude, surface=
 wave arrivals for us (at approx. 145 degrees) were obscured.  Ke=
ep up the good work.







Hi Tim,
 
Now I'm getting a bit puzzled !
 
Cheers,
 
Jorma


From: psn-l-request@webtronic= s.com [mailto:psn-l-request@............... On Behalf Of Timothy= Carpenter
Sent: 05 February 2005 21:33
To: psn-l@..............
Subject: RE: Iris Waveform Chart

I shou= ld probably know – but I don't. What is the "caustic" distance? And for that= matter, what is the "caustic"?

Regard= s,

-Tim-

 

Timothy Carpenter, P.E., Pres.,
GeoDyn= amics Consultants, Inc.
5043 Whitlow Ct.
Commerce Twp., Mi 48382
248-363-45= 29 (voice & fax)
248-766-1629 (cell)
geodynamics@........... (primary)
geodynamics@a= tt.net (secondary)

 

 

-----Original Message-----
From:= psn-l-request@.............. [mailto:psn-l-request@............... ] On Behalf Of Connie and Ji= m Lehman
Sent: S= unday, January 09, 2005 7:03 PM
To: psn-l@..............
Subj= ect: Iris Waveform Chart

 

=

PSN-= -thanks for the Iris Waveform Chart for the 9.0 Sumatra  12/26/04 event.&nbs= p; The surface wave arrivals of multiple stations exhibited by distance, and tex= t,  makes a super graphic.  I was wondering about  the occurrence= of a seismic caustic at the appropriate degree distance.  Was the gap at=20= 160 degree area due to no reporting station near the "caustic" distance.  In= periodic recording here we've copied three caustics  in 20 years--I b= elieve the events were southwest of Australia for us--not a very hot spot.

&nbs= p;   The 18 sec long period system at James Madison Un.  (Virginia) w= orking into a graphic readout read the 8.1 Macquarie Is. event-(l2/23) nicely,=20= but the 9.0 event read 20 min after P-diff arrived and then went off scale fo= r 100 minutes and returned to normal recording for the 7.1 event at 04:21. = ; One can conclude, surface wave arrivals for us (at approx. 145 degre= es) were obscured.  Keep up the good work.=

   &= nbsp;        Jim Lehman


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